An Overview of Earth History

The Earth has been around for approximately four and a half billion years! The geologic time scale is the timeline that describes all this time.

Scientists have found rocks that formed during every time period of Earth's history! In sedimentary rocks, they have found millions of fossils and clues to past environment. Take a look at the stories below to discover how some scientists are discovering more about our planet's past.

The beginning of the Eocene was a period when the Earth was very hot, with palm trees and alligators at the north pole. Earth but cooled by the start of the Quaternary. This period relates to today's concern about global warming. Homo sapiens evolved and Ice Ages occures towards the end of this time. The Little Ice Age (which is not a true ice age) occured a few hundred years ago.

The Mesozoic is the period in which the dinosaurs lived, and its end
was marked by the K-T extinction. This extinction event dramatically
changed the Earth's flora and fauna, and its causes are still being
investigated by scientists around the world. During the Mesozoic, the
giant continent Pangaea broke apart into the continents we have today.

The Cambrian period, at the beginning of the Paleozoic, was the first time that multicellular life forms florished on Earth. By the end of the Paleozoic, and beginning of the Mesozoic, all the continents of the Earth came together to form the giant continent called PANGAEA and dinosaurs began to roam on land.

This period is about 5 times as long as the Paleozoic and Mesozoic combined, a very long time. Less is known about it than the younger time periods. The oldest fossils are of bacteria/archaea dating from 3000 M. The oldest rock is dated at 3800 M. The Earth is thought to be 4600 M years old.

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